U. S. Department of Housing and Urban Development



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Wind Monitoring Approach

To achieve the objectives of this study, an industrial park in Upper Marlboro, Maryland, has been instrumented with five near-ground wind monitoring stations having anemometers at an elevation of about 10 feet (3.0 m). A typical near-ground wind station is shown in Figure 2. The five stations were located to capture a representative sample of the near-ground wind field within the built-up terrain of the industrial park. An additional monitoring station, centrally located in the industrial park, consists of two anemometers placed on a communications tower at elevations of 33 ft (10 m) and 187 ft (57 m). These two anemometers are shown in Figures 3a and 3b. Because of possible shielding and acceleration of wind for certain directions of wind, the data reported in this study for the 33-ft tower anemometer are only given for wind directions well outside the 60-degree sector of the tower frame. The anemometer at the top of the tower is located approximately 1-foot above the top rail. Its elevation above the tower was limited by FAA regulations governing the height of this particular tower.





Figure 2 - Portable near-ground wind station

with a anemometer at a 10-ft (3-m) height above ground.

Figure 3a - Lower tower anemometer

at a 33-ft (10-m) height above ground.


Figure 3b - Upper tower anemometer

at a 187-ft (57 m) height above ground.
The layout of these six stations in the industrial park is shown in the aerial photograph of Figure 4. (The tower is labeled as station #2.) As seen in the aerial photograph, the industrial park is situated in an exposure category ‘B’ environment as described by ASCE 7-95 [1]. As such, the surrounding land has both small open fields with trees on the boundaries (eastern direction) and is predominantly characterized by deciduous trees in the other directions. Within the industrial park, the buildings are typically 20 ft (6.1 m) to 30 ft (9.1 m) in height. There are also numerous parking lots and several undeveloped lots with trees, brush, and open grassy fields. The terrain is relatively flat with gently rolling hills. These conditions are similar to that found in many residential and commercial developments with a moderate density of structures.


Figure 4 - Aerial photograph of 10-ft (3-m) height wind monitoring stations

with an approximate scale of 1:8400. The tower station with anemometers at 33-ft (10-m) and 187-ft (57 m) heights is labeled as #2.

The portable near-ground wind stations have been deployed in a manner to capture different types of localized exposures within the industrial park. It is expected that, depending on wind direction, some stations will experience shielding and other possible instances of wind channeling. This realistic condition will provide highly variable readings for any given wind event across all of the wind stations, as would be expected in the interfacial layer of a suburban and wooded terrain. One of the stations (#1 in Figure 4) is located on a small knoll and may experience wind speed up due to topography for winds coming from the Northeast and Southwest. Conversely, another station (#5 in Figure 4) is located in a wooded area with a slight depression in elevation. The remaining near-ground wind stations are located in “open areas” with highly variable surroundings of buildings, parking lots, grassy lawns/fields, and woods. A detailed description of each near-ground monitoring station’s exposure is found in Table A-1 and the photographs of Appendix A.


Four of the 10-ft (3-m) near-ground stations and the tower station were instrumented with R.M. Young Wind Monitor (model 05103) directional vane anemometers and a Campbell Scientific CR-10 data-logger. This anemometer was selected because of its durability and combined ability to monitor wind speed and direction. The propeller has a threshold wind speed sensitivity of 2 mph (0.89 m/s) and a directional sensitivity of 2.2 mph (0.98 m/s) for a 10 degree displacement. One of the near-ground stations was instrumented with a Met One (model 034A-L) cup-type anemometer and a separate wind direction vane. The Met One has a wind speed threshold of 0.9 mph (0.04 m/s) and is not sensitive to wind directional changes as are vane-type anemometers. Since it was originally proposed that the portable, near-ground wind stations would also be used to capture wind-field data from a land-falling hurricane event in a residential setting, the more durable R.M. Young Wind Monitor anemometers were used on most stations.

Every monitoring station was programmed to record the following information:




  • maximum gust

  • time of maximum gust

  • direction of maximum gust

  • mean wind speed (M)

  • mean direction of mean wind

  • standard deviation of mean wind speed (S)

  • turbulence intensity in the 10-minute and 1-minute time interval of maximum gust (S/M)

Site conditions are monitored every one-second. The raw data is aggregated into one minute, five-minute, ten minute, and one-hour intervals unless the peak gust falls below 10 mph. When this occurs, only hourly data is recorded for reasons of efficiency in data storage and analysis.


Results




Selected Wind Events

This report examines near ground wind data from March 19 through April 1, 1998. During this interval wind conditions were variable but no major storms or mesocyclones occurred. The wind record is summarized for each of the five ground wind stations in the hourly maximum gust trace of Figure 5. Figure 5 shows the mean of the five ground stations’ hourly maximum gust and includes the hourly maximum gust of the 33 and 187 foot tower stations. Key data for each event and anemometer (station) is summarized in Table 1 including the following information:




  • peak wind speed for each anemometer (peak gust and maximum 1-minute, 10-minute, and hourly means),

  • wind direction at peak gust and mean wind speeds,

  • turbulence intensity (TI) at time of peak gust (1-minute and 10-minute interval),

  • gust factor (GF) for each anemometer (ratio gust to 1-minute and 10-minute mean wind speed), and

  • estimated power law exponent, , for each station and each wind speed duration based on 187-ft (57-m) measurements and either the 33-ft (10-m) tower or the five near ground 10-ft (3-m) measurements.

It should be noted in this study that the power law exponent is expressed as 1/ instead of . Therefore, the values for  represent the denominator of the power law exponent as used in the ASCE 7 standard [1].




Figure 5 - Maximum hourly gust trace for ground stations
TABLE 6
SUMMARY DATA FOR ALL WIND EVENTS DURING THE PERIOD OF RECORD

Station

Peak Gust

(mph)2



Peak 1 Min Mean

(mph)2



1 Min TI

1 Min GF

Peak 10 Min Mean

(mph)


10 Min TI

10 Min GF

1

gust


1

1 min


1

10 min


1

25.7

(NW)


18.0

(SW)


0.20

1.43

13.6

(SW)


0.25

1.89

6.12

4.93

4.89

3

27.2

(S)


18.6

(S)


0.23

1.47

12.6

(E)


0.34

2.17

6.95

5.22

4.33

4

32.2

(SW)


22.8

(SW)


0.14

1.41

17.6

(SW)


0.23

1.82

11.65

8.16

8.65

5

22.4

(S)


12.6

(S)


0.24

1.78

8.6

(S)


0.35

2.63

4.75

3.08

2.77

6

27.8

(S)


17.2

(SW)


0.25

1.61

11.8

(SW)


0.36

2.38

7.37

4.57

3.96

10’ Mean

27.1

17.9

0.21

1.54

12.9

0.31

1.96

7.371

(6.87)


5.191

(4.85)


4.921

(4.47)


10’ COV

0.13

0.20

0.21

0.10

0.25

0.20

0.21

0.351

(0.41)


0.361

(0.45)


0.451

(0.53)


33’

32.7

(S)


21.8

(SW)


0.17

1.5

14.6

(SW)


0.31

2.22

N/A

N/A

N/A

187’

41.4

(SW)


32.6

(SW)


0.10

1.27

24.8

(E)


0.20

1.67

N/A

N/A

N/A

1Based on the mean and standard deviation of the  for each of the five near ground stations. Values in parenthesis are based on the mean and standard deviation of wind speed for the five near ground stations.

21mph = 0.447 m/s.

As seen from the data, the near ground 3-second gust wind speeds varied from 22.4 mph to 32.2 mph with a COV of 0.13. When mean 1-minute and 10-minute near ground wind speeds are examined, the wind speed decreases and the COV increases as the average time interval increases, as would be expected. The turbulence intensity (TI) also varied from 0.14 to 0.25 for the 1-minute mean and 0.23 to 0.36 for the 10-minute mean. The COV of TI was similar for both average time intervals (0.21 and 0.20).


The value of  for each station is based on the maximum wind speed recorded throughout the entire reporting period. The calculation utilizes the difference in wind speeds between the 187’ and 10’ stations. Since  is being used for engineering calculations this approach represents an “extreme-value” by using only data from peak wind speeds which occurred on different times or days and wind direction between the recording stations. If the data were recorded for an entire year, the reported -values would represent an annual extreme value.



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